Dam/Barrage Year /Anne E River /Riviere City/Ville St/Et/ Pr/Dpt Type

Total Page:16

File Type:pdf, Size:1020Kb

Dam/Barrage Year /Anne E River /Riviere City/Ville St/Et/ Pr/Dpt Type Year Found Hight Vol Area Length Catc SpillCap/ River St/Et/ Type Leng Purp Type Sp Dam/barrage /Anne City/Ville /Fondatio /Haut /Vol Capacit. /Sur /Long /Bvers. E Owner/Proprie Engine/Bur.d'et Contractor/Entr /Riviere Pr/Dpt /Type /Long m /Buts /Typ Eva e n en m 103m3 103m2 km Km2 m3/s ICHIBANIKE 400 Ishite Matsuyama Ehime TE R 15 180 50 140 I 0 N Higashino Irrigation Assoc. Kagoshim Mitsumata Land SUMIYOSHIIKE 400 Beppu Gamo a TE R 20 60 14 230 I 0 N Improvement Assoc. KAERUMATAIKE 607 Yodo Nara Nara TE R 17 260 159 485 I 0 N Nara City SAYAMAIKE 616 Yamato Tondabayashi Osaka TE R 19 997 605 2800 I 18 0 N Osaka Prefecture (Obayashi-Gumi Co.) FUROTANIIKE 900 Kino Hashimoto Wakayam TE R 18 100 26 100 I 0 N Furotaniike Irrigation Wakayam Kumamichiike Irrigation KUMAMICHIIKE 900 Kino Hashimoto a TE R 18 32 5 9 I 0 N Assoc. MINENOIKE 900 Kino Hashimoto Wakayam TE R 16 45 7 15 I 0 N Minenoike Irrigation Assoc. Shido Land Improvement NAGAYUKIIKE 1000 Ohashi Takamatsu Kagawa TE R 20 171 87 483 I 0 N Assoc. Tatsuno Land DAIMONIKE 1128 Daimon Nara Nara TE X 20 78 105 98 10 I 0 N Improvement Assoc. SHINTARO 1260 Hido Ueno Mie TE 19 150 73 35 I Private Dam MARUYAMA(YAMAGU Yamaguch Maruyama Users'. CHI) 1346 Ara Ube i TE R 18 46 24 120 I 0 N Ube City Group OIKE 1360 Kino Hashimoto Wakayam TE R 18 80 30 200 I 0 N Oike Irrigation Assoc. Otaniike Land OTANIIKE 1470 Kunita Kannonji Kagawa TE R 17 304 306 928 140 I 0 N Improvement Assoc. OMINE 1480 Offstream Hikari Yamaguch TE R 16 72 16 6 I 0 N Omine Irrigation Assoc. TSUTSUMIOIKE 1500 Nuta Mihara Hiroshima TE R 15 62 30 105 I 0 N Tsutsumi Community Kozoku Land Improvement Kishu Feudal Clan Kozoku Irrigation KOZOKUIKE 1504 Kushida Matsuzaka Mie TE R 24 78 43 41 I 0 N Assoc. (defunct) Assoc. Awai Land Improvement IWANABEIKE 1530 Kunita Kannonji Kagawa TE R 16 216 68 375 I 0 N Assoc. Hirai Land Improvement DOIOKUKAMIIKE 1560 Shigenobu Matsuyama Ehime TE R 17 100 21 90 I 0 N Assoc. Hirai Land Improvement HORIKOSHIIKE 1560 Shigenobu Matsuyama Ehime TE R 16 135 26 200 I 0 N Assoc. KASUGAIKE 1560 Kino Wakayama Wakayam TE R 18 150 8 161 I 0 N Nakamitani Community Ryome Land Improvement OIKE(EHIME) 1560 Shigenobu Matsuyama Ehime TE R 15 140 28 440 I 0 N Assoc. MIIWAIKE 1580 Kigura Okayama Okayama TE 16 120 10 30 I Waki Town Masegawa Land SHIMOIKE 1580 Shibutani Matsuyama Ehime TE R 23 140 84 70 I 0 N Improvement Assoc. Iwaseike Land IWASEIKE 1592 Takase Kannonji Kagawa TE R 18 144 89 1017 I 0 N Improvement Assoc. HORIKOSHIIKE(HIRO SHIMA) 1600 Nuta Mihara Hiroshima TE R 20 72 29 96 I 0 N Hongo Town IZAWAIKE 1600 Kushida Matsusaka Mie TE R 15 100 21 90 I 0 N Awaso Community KAMISHIMOIKE 1600 Toyo Toyohashi Aichi TE R 17 30 15 I 0 N Mr. H. Kume & 94'others KAWAI NO.4 1600 Yoneshiro Odate Akita TE R 16 63 37 35 I 0 N Block of Aikawa Town Kishima Land NAGAIKEKAMI 1600 Rokkaku Saga Saga TE R 17 130 86 381 I 0 N Improvement Assoc. OIKE(NIIGATA) 1600 Hogura Naoetsu Niigata TE R 16 162 5 124 I 0 N Ikefune Community Kamitakase Land OTANIIKE(KAGAWA) 1600 Takase Kannonji Kagawa TE R 15 40 11 72 I 0 N Improvement Assoc. SEISHOIKE 1600 Hiji Ozu Ehime TE R 15 120 40 I 0 N Seishoike Irrigation Assoc. TAKAOTSUTSUMIKA 1600 Suetake Tokuyama Yamaguch TE R 17 25 6 I 0 N Sakamoto Community TAKAOTSUTSUMINA 1600 Suetake Tokuyama Yamaguch TE R 16 30 8 2 I 0 N Sakamoto Community DEGUCHI 1601 Yaishi Ube Yamaguch TE R 20 108 69 450 I 0 N Deguchi Users'. Group TAKINOOKUIKE 1602 Hiji Ozu Ehime TE R 17 150 50 I 0 N Takinookuike Irrigation AGARI 1603 Nishida Shimonoseki Yamaguch TE R 21 59 27 22 I 0 N Mr. M. Harada AKASAKA(WAKAYAM 1603 Kino Hashimoto Wakayam TE R 17 85 16 49 I 0 N Akasaka Irrigation Assoc. ANAIKE 1603 Hidaka Gobo Wakayam TE R 18 45 28 181 I 0 N Anaike Users' Group BANTODAME 1603 Hijie Inabe Mie TE R 20 120 77 73 I 0 N Bantodame Users' Group BUNKAIKE 1603 Ishi Tondabayashi Osaka TE R 15 54 12 24 I 0 N Taishi Town Musaho Community CHIGAIGADANIIKE 1603 Iwamatsu Uwajima Ehime TE R 19 70 12 25 I 0 N (Tsushima Town) DABAIKE 1603 Hiji Ozu Ehime TE R 15 150 42 I 0 N Dabaike Irrigation Assoc. Noma Land Improvement FURUIKE 1603 Takuma Imabari Ehime TE R 17 70 30 40 I 0 N Assoc. Matsuyukikami Irrigation FURUIKE(OITA) 1603 Katsura Bungo-takada Oita TE R 17 94 18 17 I 0 N Assoc. Futamatakamiike Land FUTAMATAKAMIIKE 1603 Shin Takamatsu Kagawa TE R 17 280 148 606 I 0 N Improvement As GANBUCHIIKE 1603 Akashi Kobe Hyogo TE R 19 82 58 39 I 0 N Mr. T. Fujimoto GOROGAEKI 1603 Koto Ube Yamaguch TE R 15 30 I 0 N Kurokawa Community HACHIOJI 1603 Muko Fukuchiyama Hyogo TE R 17 55 31 32 I 0 N Mr. T. Fujiwara HARA 1603 Inunaki Nogata Fukuoka TE R 18 53 25 I 0 N Wakayama Town HARAGUCHI 1603 Osano Fukuoka Fukuoka TE R 18 100 4 I 0 N Dazaifu Town Dazaifu Town Dazaifu Town HATAIKE 1603 Offstream Okayama Okayama TE R 23 124 80 176 I 0 N Okayama City Hataike Users' Group Year Found Hight Vol Area Length Catc SpillCap/ River St/Et/ Type Leng Purp Type Sp Dam/barrage /Anne City/Ville /Fondatio /Haut /Vol Capacit. /Sur /Long /Bvers. E Owner/Proprie Engine/Bur.d'et Contractor/Entr /Riviere Pr/Dpt /Type /Long m /Buts /Typ Eva e n en m 103m3 103m2 km Km2 m3/s Honsho Community, Honsho Community, HATTAIKE 1603 Shin Imabari Ehime TE R 16 55 21 50 I 0 N Yoshiumi Town Yoshiumi Town HAYASHITANIIKE 1603 Kako Miki Hyogo TE R 20 55 39 49 I 0 N Mr. A. Fujimoto Higashino Land Higashino Land HIGASHINO 1603 Kiso Ena Gifu TE R 25 168 98 758 I 0 N Improvement Assoc. Gifu Prefecture Improvement Assoc. HIGASHITANIIKE(EHI Kitagata (kawauchi Town) ME) 1603 Hosen Matsuyama Ehime TE R 21 67 33 28 I 0 N Land HIGETANIIKE 1603 Kako Kobe Hyogo TE R 17 51 29 68 I 0 N Mr. N. Sakamoto HIKAKETAMEIKE 1603 Ono Mie Oita TE R 16 69 20 I 0 N Kamitahara Community HIMUJITAMEIKE 1603 Ono Mie Oita TE R 16 43 21 17 I 0 N Assamizu Community Sugao Village HIRAOIKE 1603 Jizoin Nara Nara TE R 16 230 69 96 I 0 N Nara City ICHIGAEKI 1603 Kanda Shimonoseki Yamaguch TE R 15 43 15 25 I 0 N Mr. K. Uemura North Fuwa District Land IKEDERA 1603 Makita Ogaki Gifu TE R 20 150 40 205 I 0 N Improvemen IKENOJIRI 1603 Osano Fukuoka Fukuoka TE R 18 58 11 I 0 N Dazaifu Town IMOGATANIIKE 1603 Kako Miki Hyogo TE R 25 35 10 23 I 0 N Mr. K. Sugiura Ippodani Land IPPODANIIKE 1603 Yoshii Tsuyama Okayama TE R 17 16 25 64 I 0 N Improvement Assoc. Nishisachi Community Wakimoto Land IWAKURASAWA 1603 Offstream Oga Akita TE R 16 144 48 240 I 0 N Improvement Assoc. Akita Prefecture IWATANIIKE 1603 Nabano Aioi Hyogo TE R 20 77 44 280 I 0 N Nabano Community Hyogo Prefecture JIGOKUDANIIKE 1603 Noto Nara Nara TE R 15 200 17 90 I 0 N Nara Prefecture JINGOROIKE 1603 Yodo Nara Nara TE R 15 120 68 650 I 0 N Nara City JODOJI 1603 Ano Tsu Mie TE R 16 60 100 I 0 N Jodoji Community Ikeda Feudal Clan Ikeda Feudal Clan JOGAHATASHIMOIKE 1603 Yoshii Okayama Okayama TE R 20 60 8 320 I 0 N Yoshinaga Town (defunct) (defunct) Wakayam Juji-Nakasakontameike JUJIIKE 1603 Kino Wakayama a TE R 16 420 33 360 I 0 N Land Improvem Kitaura-ichinomekata Land KAITAZAWA 1603 Nomura Oga Akita TE R 15 40 21 300 I 0 N Improveme Akita Prefecture KAKOGAIKE 1603 Tenpaku Nagoya Aichi TE R 20 172 381 54 I 0 N Odaka Town KANMORIKOJIIKE 1603 Asahi Okayama Okayama TE R 19 90 31 50 I 0 N Tsudaka Town KARATACHIIKE 1603 Miwatari Matsuzaka Mie TE R 17 163 63 57 I 0 N Karatachiike Irrigation Kasadaodame Land Matsudaira Feudal Clan Matsudaira Feudal Clan KASADAODAME 1603 Akechi Inabe Mie TE R 15 800 125 486 I 0 N Improvement Assoc. (defunct) (defunct) Kitadani Land KITADANIIKE 1603 Kushida Matsuzaka Mie TE R 17 146 42 138 I 0 N Improvement Assoc. Kamitahara Land KITAOTANIIKE 1603 Yodo Neyagawa Osaka TE R 18 58 21 60 I 0 N Improvement Assoc. KOCHIGAEKI 1603 Koya Shimonoseki Yamaguch TE R 20 110 180 I 0 N Mr. K. Okamoto Kochigaeki Users' KOYADANIIKE(HYOG 1603 Kako Miki Hyogo TE R 16 62 26 I 0 N Mr. J. Inoue Wakami Community KOYAMADAIKE 1603 Ikejiri Toyohashi Aichi TE R 24 110 I 0 N (Akabane Town) Wakami Community KOYASHIKI 1603 Honami Iizuka Fukuoka TE R 15 75 60 100 I 0 N Chikuho Town KURATANIIKE 1603 Kino Hashimoto Wakayam TE R 28 80 26 120 I 0 N Kurataniike Irrigation KUREKOSHIIKE 1603 Tatsue Komatsujima Tokushim TE R 28 102 54 92 I 0 N Kushibuchi Irrigation KUROISHIIKE 1603 Yoshioka Kurashiki Okayama TE R 15 85 28 125 I 0 N Kurashiki City Momoeda Community (Mie KUROIWATAMEIKE 1603 Ono Mie Oita TE R 16 111 42 40 I 0 N Town) KUSABA 1603 Kusaba Shimonoseki Yamaguch TE R 15 60 17 27 I 0 N Mr.
Recommended publications
  • Premium Wagyu History Nature
    Matsusaka City Guide Nature Premium Wagyu History Matsusaka City Matsusaka is located in Mie Prefecture, near the center of Japan. With the sea to the east and mountains in the west, Matsusaka’s gorgeous natural scenery is a joy in every season. World-famous Matsusaka Cattle are raised right here in the city. Matsusaka, where history and culture blend Matsusaka City Tourist into peoples’ everyday lives, is the perfect 1 2 Matsusaka Cotton Center Information Center 松阪もめん手織りセンター place to enjoy with a leisurely stroll around 豪商のまち松阪 観光交流センター This center works to hand down knowledge about the traditional On the first floor you can get information on sightseeing handicraft Matsusaka Cotton. Fabric, kimono, and accessories on town. and places to eat in Matsusaka. There are also many sale all feature a beautiful indigo striped pattern, and make excellent souvenirs and special products of Matsusaka for sale. The souvenirs. Also popular with customers is the authentic Edo-period second floor introduces the history of Matsusaka through a loom, which you can use to hand-weave the fabric yourself. video playing in the theatre room (with English subtitles) and an exhibit of informational panels. This facility is a great place to start exploring Matsusaka City. Matsusaka IC 0 100 200 300m Matsusaka Agricultural Park Bell Farm 12 4 Former Ozu Residence Motoori Norinaga Matsusaka City (Matsusaka Merchant Museum) Memorial Museum/ Cultural Asset Center Former Hasegawa Residence 10 Suzu-no-Ya "Haniwa Museum" 3 旧小津清左衛門家 8 本居宣長記念館・鈴屋 旧長谷川治郎兵衛家 ATM This is the former residence of Ozu Seizaemon, a 166 The Hasegawa family made its fortune as cotton Castle Guard Matsusaka Castle successful merchant who traded paper and cotton on a Residences 7 merchants in Edo (now Tokyo).
    [Show full text]
  • Biogeography and Evolution of the Carassius Auratus-Complex in East
    Takada et al. BMC Evolutionary Biology 2010, 10:7 http://www.biomedcentral.com/1471-2148/10/7 RESEARCH ARTICLE Open Access Biogeography and evolution of the Carassius auratus-complex in East Asia Mikumi Takada1,2*, Katsunori Tachihara1, Takeshi Kon2, Gunji Yamamoto2, Kei’ichiro Iguchi3, Masaki Miya4, Mutsumi Nishida2 Abstract Background: Carassius auratus is a primary freshwater fish with bisexual diploid and unisexual gynogenetic triploid lineages. It is distributed widely in Eurasia and is especially common in East Asia. Although several genetic studies have been conducted on C. auratus, they have not provided clear phylogenetic and evolutionary descriptions of this fish, probably due to selection bias in sampling sites and the DNA regions analysed. As the first step in clarifying the evolutionary entity of the world’s Carassius fishes, we attempted to clarify the phylogeny of C. auratus populations distributed in East Asia. Results: We conducted a detailed analysis of a large dataset of mitochondrial gene sequences [CR, 323 bp, 672 sequences (528 sequenced + 144 downloaded); CR + ND4 + ND5 + cyt b, 4669 bp in total, 53 sequences] obtained from C. auratus in East Asia. Our phylogeographic analysis revealed two superlineages, one distributed mainly among the Japanese main islands and the other in various regions in and around the Eurasian continent, including the Ryukyus and Taiwan. The two superlineages include seven lineages with high regional specificity that are composed of endemic populations indigenous to each region. The divergence time of the seven lineages was estimated to be 0.2 million years ago (Mya) by a fossil-based method and 1.0-1.9 Mya by the molecular clock method.
    [Show full text]
  • Muko City, Kyoto
    Muko city, Kyoto 1 Section 1 Nature and(Geographical Environment and Weather) 1. Geographical Environment Muko city is located at the southwest part of the Kyoto Basin. Traveling the Yodo River upward from the Osaka Bay through the narrow area between Mt. Tenno, the famous warfield of Battle of Yamazaki that determined the future of this country, and Mt. Otoko, the home of Iwashimizu Hachimangu Shrine, one of the three major hachimangu shrines in Japan, the city sits where three rivers of the Katsura, the Uji and the Kizu merge and form the Yodo River. On west, Kyoto Nishiyama Mountain Range including Mt. Oshio lays and the Katsura River runs on our east. We share three boundaries with Kyoto city - the northern and western boundaries with Nishikyo-ku, and the eastern boundary with Minami-ku and Fushimi-ku. Across the southern boundary is Nagaokakyo city abutting Oyamazaki-cho which is the neighbor of Osaka Prefecture. The city is approximiately 2km from east to west and approximiately 4km from south to north covering the 7.72km2 area. This makes us the third smallest city in Japan after Warabi city and Komae city. Figure 1-1-1 Location of Muko city (Right figure (Kyoto map) : The place of red is Muko city) (Lower figure (Japan map) : The place of red is Kyoto) N W E S 1 Geographically, it is a flatland with the northwestern part higher and the southwestern part lower. This divides the city coverage into three distinctive parts of the hilly area in the west formed by the Osaka Geo Group which is believed to be cumulated several tens of thousands to several million years ago, the terrace in the center, and the alluvial plain in the east formed by the Katsura River and the Obata River.
    [Show full text]
  • Studies on the Genesis of Metallic Mineral Deposits of Shin Jo and Yamagata Basins, Northeastern Japan (I)
    岩 石鉱 物鉱 床学 会誌 60巻4号, 1968年 STUDIES ON THE GENESIS OF METALLIC MINERAL DEPOSITS OF SHIN JO AND YAMAGATA BASINS, NORTHEASTERN JAPAN (I) NORITSUGU OIZUMI Mining Division Prefectuval Governient of Yamagata The present structural set up of the Shinjo and Yamagata basins which are situated within the Inner Region, Northeastern Japan, is a result of repeated uplift and submergence coupled with igneous activity and sedimentation during the early stage of the Neogene. Those structur es formed as a result of uplift of the basement are the major faults and fissures parallel to the N-S trend of the present axis of the Basement Rise and the subordinate faults and fissures trending E-W and perpen dicular to that axis Those formed as a result of folding of the sedimentary rocks are the NNW-SSE trending structures of northern Shinjo Basin, the N-S trending structures of southern Shinjo Basin, the N-S trending structures of northern Yamagata Basin, and the NNE-SSW trending structures of southern Yamagata Basin. These structures include the fold axes and the faults and fissures parallel to them. In addition to these structures produced by folding of the sedimentary rocks, are the subordinate faults and fissures trending WNW and NE-SW to ENE. The crushed zones within these fractures were produced by an E-W lateral compression, which also produced exceedingly abundant E-W trending tension fractures, The NNE-SSE trending fissures adhere closely to these fractures caused by lateral compression. The individual ore deposits present within the two basins amount to a total of more than 300 ore deposits.
    [Show full text]
  • Japan Geoscience Union Meeting 2009 Presentation List
    Japan Geoscience Union Meeting 2009 Presentation List A002: (Advances in Earth & Planetary Science) oral 201A 5/17, 9:45–10:20, *A002-001, Science of small bodies opened by Hayabusa Akira Fujiwara 5/17, 10:20–10:55, *A002-002, What has the lunar explorer ''Kaguya'' seen ? Junichi Haruyama 5/17, 10:55–11:30, *A002-003, Planetary Explorations of Japan: Past, current, and future Takehiko Satoh A003: (Geoscience Education and Outreach) oral 301A 5/17, 9:00–9:02, Introductory talk -outreach activity for primary school students 5/17, 9:02–9:14, A003-001, Learning of geological formation for pupils by Geological Museum: Part (3) Explanation of geological formation Shiro Tamanyu, Rie Morijiri, Yuki Sawada 5/17, 9:14-9:26, A003-002 YUREO: an analog experiment equipment for earthquake induced landslide Youhei Suzuki, Shintaro Hayashi, Shuichi Sasaki 5/17, 9:26-9:38, A003-003 Learning of 'geological formation' for elementary schoolchildren by the Geological Museum, AIST: Overview and Drawing worksheets Rie Morijiri, Yuki Sawada, Shiro Tamanyu 5/17, 9:38-9:50, A003-004 Collaborative educational activities with schools in the Geological Museum and Geological Survey of Japan Yuki Sawada, Rie Morijiri, Shiro Tamanyu, other 5/17, 9:50-10:02, A003-005 What did the Schoolchildren's Summer Course in Seismology and Volcanology left 400 participants something? Kazuyuki Nakagawa 5/17, 10:02-10:14, A003-006 The seacret of Kyoto : The 9th Schoolchildren's Summer Course inSeismology and Volcanology Akiko Sato, Akira Sangawa, Kazuyuki Nakagawa Working group for
    [Show full text]
  • Toyama Bay, Japan
    A Case Study Report on Assessment of Eutrophication Status in Toyama Bay, Japan Northwest Pacific Region Environmental Cooperation Center July 2011 Contents 1. Scope of the assessment........................................................................................................................................................... 1 1.1 Objective of the assessment .................................................................................................................................... 1 1.2 Selection of assessment area................................................................................................................................... 1 1.3 Collection of relevant information.......................................................................................................................... 3 1.4 Selection of assessment parameters........................................................................................................................ 4 1.4.1 Assessment categories of Toyama Bay case study ....................................................................................4 1.4.2 Assessment parameters of Toyama Bay case study...................................................................................4 1.5 Setting of sub-areas .................................................................................................................................................. 4 2. Data processing........................................................................................................................................................................
    [Show full text]
  • This Data Sheet Compiles Individual Test Results Shown in Corresponding
    Levels of radioactive contaminants in foods (data reported on 20 Sep 2011) Note: This data sheet compiles individual test results shown in corresponding press release written in Japanese, available at http://www.mhlw.go.jp/stf/houdou/bukyoku/iyaku.html Food origin Level of radioactive contaminants in food Press release date Sampling date Food tested (expressed as radionuclide levels (Bq/kg)). Prefecture Area Iodine‐131 Cesium‐134 Cesium‐137 1 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 2 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 3 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 4 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 5 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 6 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 7 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 8 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 9 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 10 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND 101.6 11 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 12 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 13 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 14 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 15 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 16 20‐Sep‐11 Miyagi Kawasaki‐machi 17‐Sep‐11 rice (outdoor) ND ND 17 20‐Sep‐11 Miyagi Kawasaki‐machi 17‐Sep‐11 rice (outdoor) ND ND 18 20‐Sep‐11 Miyagi
    [Show full text]
  • Geomorphological Evolution and Sediment Budget Analysis with the Uji River, Kyoto
    D-7 Fourth International Conference on Scour and Erosion 2008 GEOMORPHOLOGICAL EVOLUTION AND SEDIMENT BUDGET ANALYSIS WITH THE UJI RIVER, KYOTO Ryoukei AZUMA1 and Hideo SEKIGUCHI2 1Member of ISSMGE, Assistant Professor, Disaster Prevention Research Institute, Kyoto University (Shimomisu, Yoko-oji, Fushimi-ku, Kyoto 612-8235, Japan) E-mail:[email protected] 2 Member of ISSMGE, Professor, Disaster Prevention Research Institute, Kyoto University (Shimomisu, Yoko-oji, Fushimi-ku, Kyoto 612-8235, Japan) E-mail:[email protected] This paper starts with presenting field evidences that illustrate the occurrence of significant bank erosion in a reach of the Uji River. It then demonstrates that the resulting escarpment was not a mere local adjustment, but is an indicator as to how extensively the Uji River has undergone appreciable amounts of channel erosion over the entire 15.2km-long section. The datasets on which the discussion is based include: the cross-channel topographical data (200m intervals along the river course) in 1967, 1979 and 2006 made available from the Yodogawa Office, MLIT. A careful geomorphological analysis of the datasets in terms of GIS, permitted the determination of tempo-spatial changes of areal sediment storage in the Uji River. When integrated over the entire river course, the overall volume of sediment loss due to erosion proved to amount to 3.1 ×106 m3 in the period from 1967 up to 2006. A discussion is made to identifying its practical implications for future riverine management. Furthermore, a discussion is made of the linkage between the extent of the channel erosion and the depositional environments of the sediment that constitutes the boundary of the river channel.
    [Show full text]
  • Flood Loss Model Model
    GIROJ FloodGIROJ Loss Flood Loss Model Model General Insurance Rating Organization of Japan 2 Overview of Our Flood Loss Model GIROJ flood loss model includes three sub-models. Floods Modelling Estimate the loss using a flood simulation for calculating Riverine flooding*1 flooded areas and flood levels Less frequent (River Flood Engineering Model) and large- scale disasters Estimate the loss using a storm surge flood simulation for Storm surge*2 calculating flooded areas and flood levels (Storm Surge Flood Engineering Model) Estimate the loss using a statistical method for estimating the Ordinarily Other precipitation probability distribution of the number of affected buildings and occurring disasters related events loss ratio (Statistical Flood Model) *1 Floods that occur when water overflows a river bank or a river bank is breached. *2 Floods that occur when water overflows a bank or a bank is breached due to an approaching typhoon or large low-pressure system and a resulting rise in sea level in coastal region. 3 Overview of River Flood Engineering Model 1. Estimate Flooded Areas and Flood Levels Set rainfall data Flood simulation Calculate flooded areas and flood levels 2. Estimate Losses Calculate the loss ratio for each district per town Estimate losses 4 River Flood Engineering Model: Estimate targets Estimate targets are 109 Class A rivers. 【Hokkaido region】 Teshio River, Shokotsu River, Yubetsu River, Tokoro River, 【Hokuriku region】 Abashiri River, Rumoi River, Arakawa River, Agano River, Ishikari River, Shiribetsu River, Shinano
    [Show full text]
  • Source Apportionment of Annual Water Pollution Loads in River Basins by Remote-Sensed Land Cover Classification
    water Article Source Apportionment of Annual Water Pollution Loads in River Basins by Remote-Sensed Land Cover Classification Yi Wang 1, Bin He 2,*, Weili Duan 2,*, Weihong Li 1, Pingping Luo 3,4 and Bam H. N. Razafindrabe 5 1 State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; [email protected] (Y.W.); [email protected] (W.L.) 2 Key Laboratory of Watershed Geographic Science, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China 3 Key Laboratory of Subsurface Hydrology and Ecological Effects in Arid Region (Chang’an University), Ministry of Education, Xi’an 710064, China; [email protected] 4 School of Environmental Science and Engineering, Chang’an University, Xi’an 710064, China 5 Faculty of Agriculture, University of the Ryukyus, Nishihara, Okinawa 903-0213, Japan; [email protected] * Correspondence: [email protected] (B.H.), [email protected] (W.D.); Tel.: +86-025-8688-2171 (B.H.); +86-025-8688-2173 (W.D.) Academic Editor: Y. Jun Xu Received: 4 April 2016; Accepted: 9 August 2016; Published: 23 August 2016 Abstract: In this study, in order to determine the efficiency of estimating annual water pollution loads from remote-sensed land cover classification and ground-observed hydrological data, an empirical model was investigated. Remote sensing data imagery from National Oceanic and Atmospheric Administration (NOAA) Advanced Very High Resolution Radiometer were applied to an 11 year (1994–2004) water quality dataset for 30 different rivers in Japan.
    [Show full text]
  • What Is Dewa Sanzan? the Spiritual Awe-Inspiring Mountains in the Tohoku Area, Embracing Peopleʼs Prayers… from the Heian Period, Mt.Gassan, Mt.Yudono and Mt
    The ancient road of Dewa Rokujurigoegoe Kaido Visit the 1200 year old ancient route! Sea of Japan Yamagata Prefecture Tsuruoka City Rokujurigoe Kaido Nishikawa Town Asahi Tourism Bureau 60-ri Goe Kaido Tsuruoka City, Yamagata Prefecture The Ancient Road “Rokujuri-goe Kaido” Over 1200 years, this road has preserved traces of historical events “Rokujuri-goe Kaido,” an ancient road connecting the Shonai plain and the inland area is said to have opened about 1200 years ago. This road was the only road between Shonai and the inland area. It was a precipitous mountain road from Tsuruoka city to Yamagata city passing over Matsune, Juo-toge, Oami, Sainokami-toge, Tamugimata and Oguki-toge, then going through Shizu, Hondoji and Sagae. It is said to have existed already in ancient times, but it is not clear when this road was opened. The oldest theory says that this road was opened as a governmental road connecting the Dewa Kokufu government which was located in Fujishima town (now Tsuruoka city) and the county offices of the Mogami and Okitama areas. But there are many other theories as well. In the Muromachi and Edo periods, which were a time of prosperity for mountain worship, it became a lively road with pilgrims not only from the local area,but also from the Tohoku Part of a list of famous places in Shonai second district during the latter half of the Edo period. and Kanto areas heading to Mt. Yudono as “Oyama mairi” (mountain pilgrimage) custom was (Stored at the Native district museum of Tsuruoka city) booming.
    [Show full text]
  • 資料29-4 Ihpトレーニングコース2014概要,2013
    International Hydrological Programme International Hydrological Programme Forest Hydrology Conservation of Forest, Soil, and Water Resource The Twenty-fourth IHP Training Course 24 November - 7 December, 2014 Nagoya, Japan Hydrospheric Atmospheric Research Center, Nagoya University Supported by Water Resources Research Center, Disaster Prevention Research Institute, Kyoto University Outline A short training course “Forest Hydrology Conservation of Forest, Soil, and Water Resource” will be programmed for participants from Asia-Pacific regions as a part of Japanese contribution to the International Hydrological Program (IHP). The course is composed of a series of lectures and practice sessions. Objectives Incident rainwater is firstly intercepted by foliage and branches and evaporates from their surface to the atmosphere. From the surface full of rainwater, the rainwater conducts to soils along the plant body, and also, some of incident rainwater directly reaches the soils without touching foliage and branches. These rainwaters coming to the soils infiltrate into the soils with being influenced by the soil pore structure, and reaching to groundwater table. During the slow soil water movement, some of the soil water is absorbed by plant roots. It conducts through stem conduits, reaches leaves, and evaporates to the atmosphere through stomata. The ground water flows to a river. This is an outline of water cycling in the forest ecosystems, and science on this water cycling is “Forest Hydrology”. As one can see above, Forest Hydrology has two major scientific aspects, i.e., discharge from forested watershed and water use by trees (evaporation from the forest canopy). Soils in the forested watershed have a high hydraulic conductivity at the ground surface, which prevents from soil erosion, and functions to make soil water flow slow, resulting in a behavior like a dam.
    [Show full text]